Stream food webs in tropical mountains rely on allochthonous carbon regardless of land use.

The relative importance of allochthonous and autochthonous carbon (C) as sources of energy for tropical stream food webs remains an open question. Allochthonous C might be the main energy source for small and shaded forest streams, while autochthonous C is more likely to fuel food webs draining land uses with less dense vegetation. We studied food webs in cloud forest streams draining watersheds with forests, coffee plantations, and pastures. Our goal was to assess the effects of those land uses on the C source and structure of stream food webs. The study took place in tropical montane streams in La Antigua Watershed, in eastern Mexico. We selected three streams per land use and sampled biofilm and leaf litter as the main food resources, and macroinvertebrates and aquatic vertebrates from different trophic guilds. Samples were analyzed for δ13C and δ15N isotopes. Using a Bayesian mixing model, we estimated the proportional assimilation of autochthonous and allochthonous carbon by each guild. We found that consumers were mostly using allochthonous C in all streams, regardless of watershed land use. Our findings indicate that montane cloud forest streams are dominated by allochthony even in watersheds dominated by pastures. Abundant precipitation in this life zone might facilitate the movement of allochthonous C into streams. While food webs of streams from coffee plantations and pastures also rely on allochthonous resources, other impacts do result in important changes in stream functioning.

Osteoinduction in the palatal submucosa by injecting BMP-2 on 2 different carriers.

In this work, we investigated the ability of injected recombinant human bone morphogenetic protein 2 (rhBMP-2) on brushite cement (a ß-tricalcium phosphate-based biomaterial) and collagen gel as carriers to induce osteogenic differentiation in the palatal submucosa of 10-day-old rats. This was part of a broader study aiming to create bone in the palatal submucosa at cleft palate edges in the search for a minimally invasive treatment. Thirteen treated animals, 7 with rhBMP-2/brushite cement and 6 with rhBMP-2/collagen gel, were injected with 5 to 10 µL of each biomaterial in the right palatal submucosa at the level between the second and third rugae. The contralateral site was uninjected and served as the control. Six weeks after injection, both brushite cement and collagen gel were histologically unrecognizable in all treated animals. New bone structures such as ossicles of woven bone were not detected. However, an augmentation in the thickness of the palatal fibromucosa was observed at the injection site of all palates. In addition, immunolabeling for osteopontin, proliferating cell nuclear antigen, and TUNEL revealed intense osteogenic induction at the injection site with both constructs, which was negative in the control site from the same specimens; no differences regarding cell proliferation and death were observed. The present study confirms the feasibility of generating osteogenic cells in the palatal submucosa by injecting low doses of rhBMP-2 in these 2 biomaterials, together with their inability to form bone.